Water under Columbiana County comes from old shale and sandstone rock layers that formed hundreds of millions of years ago. These layers have tiny cracks and spaces where groundwater collects and moves very slowly. The rock itself holds water, but the water quality depends on what the rock contains and what the water touches as it sits underground.
Lead, manganese, iron, and sulfate come straight from the rock. These old shale layers contain coal seams and iron-bearing minerals that dissolve into water over time. Chloride and sulfate also come from salt deposits buried deep in these rock layers. The slow movement of water through tight cracks means contaminants have plenty of time to dissolve into the groundwater before reaching your well.
This water is extremely hard and loaded with minerals. The high sodium and sulfate levels mean scale buildup will coat your pipes, fixtures, and water heater. Iron at these concentrations will stain sinks and laundry orange-brown and give the water a metallic taste. You need a water softener paired with an iron filter to make this water usable for daily life.
Lead exceeds EPA health standards in Columbiana County well water. Iron and manganese also exceed their health limits. These metals come from the coal-bearing rock layers under your area and dissolve into groundwater naturally. This is a high-urgency situation that needs immediate attention.
Long-term exposure to elevated lead harms brain development in children and can damage kidneys and the nervous system in adults. Manganese exposure can hurt learning and behavior. Iron at these extreme levels will stain your sinks, toilets, and laundry orange-brown and will damage appliances. Your water is extremely hard and will leave thick scale buildup on pipes and fixtures.
Get your well tested by a state-certified lab right away. A basic health screen runs $50–100. A comprehensive metals panel runs $200–400 and is strongly recommended given the multiple contaminants. A whole-house treatment system combining water softening, iron filtration, and carbon filtration can address these issues.
| Contaminant | Samples ⓘ | % Above MCL ⓘ | Distribution ⓘ | Confidence ⓘ | Risk ⓘ |
|---|---|---|---|---|---|
| Lead | 7 | 100% | 14% · 0% · 86% | Low | High |
| Manganese | 20 | 90% | 5% · 10% · 85% | Moderate | High |
| Iron | 99 | 68% | 21% · 11% · 68% | Moderate | High |
| Chloride | 83 | 37% | 55% · 8% · 36% | Moderate | High |
| Sulfate | 72 | 33% | 53% · 14% · 33% | Moderate | High |
| Arsenic | 5 | 0% | 80% · 20% · 0% | Low | Low |
| Fluoride | 17 | 0% | 100% · 0% · 0% | Moderate | Low |
| Nitrite | 28 | 0% | 96% · 4% · 0% | Moderate | Low |
| Uranium | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Sodium | 59 | — | — | Moderate | Low |
| pH | 14 | — | — | Low | Low |
| Nitrate | 1 | — | — | Low | Safe |
| Nitrate | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Hardness | 41 | — | — | Moderate | Low |
| Fecal Coliform | 1 | — | — | Low | Safe |
MCL = Maximum Contaminant Level (EPA limit for public water; used as benchmark for private wells). Distribution shows % of sampled wells in each concentration band. Methodology.
Population-level CDC data. Not individual risk prediction.
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